The Brombachsee Marathon began at Lake Brombach and ended in Pleinfeld. The district's respiratory protection middle is positioned on the positioning of the Pleinfeld fireplace brigade. The majority of the southern part of the catchment area is located in the adjoining natural area of ​​the southern Franconia alb, together with the higher Rezattal and the low hill and mountain nation east of it in the sub-space of ​​the Weißenburger Alb, whereas the areas on the left and west of the valley belong to the underground Weimersheimer Platte. It rises right here in a short facet valley in the Narche Altmühlalb natural space of ​​her north -wing important valley, which additionally units the Altmühl flowing to the valley axis on the facet of the valley axis. That is where the valley begins to deepen. From there up to the mouth, the valley and the rest of the precise-hand catchment space belong to the sub-area Rother Sand Platten, whereas the left-hand catchment space is distributed over the sub-areas Southern Foreland of the Spalt Hill Nation (with Brombachgrund) within the south, Southern Spalt Hill Country within the northwest and north and a span of the Eastern Foreland of thespalter hill nation near the mouth of the Rezat to the left. It is surrounded by forests in a valley that opens to the east. NHN between Muhr am See in the southeast and Ornbau in the northwest and is bordered in the south by the Altmühlsee, in the east by the Mönchswald, in the north by the towns of Hirschlach and Heglau and within the west by the Altmühlzuleiter.

Just behind Weißenburg, its longest tributary, the Felchbach, reaches it from the east. From Galgenberg to the Kingdom of Heaven (Weißenburg Native Historical past Books Quantity 4), Weißenburg i. ↑ Ulf Beier: Weißenburg field name guide. ↑ Ralph Jätzold: Geographical survey of the nation: The pure spatial models on sheet 172 Nördlingen. ↑ Alexander von Humboldt Professorship|Friedrich Alexander College Erlangen-Nuremberg. ↑ Johann Alexander Döderlein: Schediasma Historicum, IMPP. Johann Kaspar Bundschuh: Retzat. " in a doc, they in all probability first sat on the stone house outside the village and in the course of the twelfth or 13th century they moved their headquarters to the moated castles inside the village. NN the Hornauer Weiher on the sting of the village of Hornau, approx. The drain from The remains of the canal results in the Altmühl. At the locks on the south ramp of the primary-Danube Canal - Kelheim, Riedenburg, Dietfurt, Berching and Bachhausen - pumping stations with a delivery capacity of 35 m³/s are put in, which provide both the canal's water provide and serve as a transition. → Exit of the Jochsberger Mühlkanal, to the fitting at 426 m above Furthgraben, from the correct and west to over 426 m above sea level. It initially runs by way of the flat Ried after which passes the core town of Weissenburg in the west. From a natural perspective, the catchment space there shares the eaves of the southern Franconian Alb, and extra precisely, its sub-areas (from southwest to northeast) Weißenburger Alb, Anlauteralb and Anlauter-Braunjuratrichter.

Lastly, the Swabian Rezat unites between the eponymous foremost city of the municipality of Georgensgmünd on the left and its district of Petersgmünd on the suitable opposite at an altitude of 341.7 m with the Franconian Rezat, which comes from the southwest and is for much longer and has a richer catchment area, to kind the oblique Foremost tributary Rednitz. Based on tradition, Charlemagne already needed to overcome the primary European watershed between the catchment areas of the Danube and Rhine, which runs, amongst other issues, over the mountain ranges between the Swabian Rezat and Altmühl, through a canal. Then straight again into open move, it passes the Letzleinsmühle on the correct bank, now flows north between the Galgenberg on the correct and the final wasteland of Simonsmühle von Gnotzheim on the left and then modifications to the city limits of Gunzenhausen just below the hamlet of Steinacker on the fitting slope. After descending from the Alb plateau, the Scheide strikes, initially over the Franconian Alb-Zeugenberg Schloßberg (606.7 m), in front of, amongst other things, the tributaries of the upper Roth approximately northwest to the confluence with the Franconian Rezat; Here the catchment area of ​​the Rednitz borders on the skin. The northern watershed west of the mouth borders the decrease catchment space of ​​the Franconian Rezat, which also competes in the northwest via its proper-hand tributary Erlbach close to Höfstetten.

The more important tributaries of the Swabian Rezat, listed from origin to confluence. There are a number of green areas in Pleinfeld, particularly alongside the Swabian Rezat, which are characterized by broad meadows and small bridges. No federal waterways run by means of Pleinfeld as a result of no river in the region is appropriate for delivery. ↑ Joshua Sans: Cheers to the region. ↑ Names of our bodies of water within the Weißenburg-Gunzenhausen district, Mfr., in: Sheets for Upper German name research. It then takes up the Brombach coming from the Großer Brombachsee and passes several mills and the villages of Mühlstetten and Niedermauk, two districts of the municipality of Röttenbach in the Roth district. Massive parts of the southern and jap half of the municipality are occupied by a forestless open landscape. With a vertical Kaplan turbine with a circulation rate of 14 m³/s and a head of 7.20 m, an electrical output of 898 kW is achieved; the system has a regular output of 1.Eight GWh per year. From 60 m³/s one speaks of a 100-year flood at the Swabian Rezat. It belongs to the river system of the Rhine and is the less water -wealthy of the two source rivers of the Rednitz - its left and western supply circulate is the longer and water -rich Franconian recurrence - hydrographically, a tribute to the Rednitz. NHN Excessive summit of the leaf bichel east of the Wülzburg on the southeastern water sheath.

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